Abstract
Abstract. The reaction of isoprene (C5H8) with hydroxyl radicals has been studied in the absence of nitrogen oxides (NOx) to determine physical and chemical characteristics of the secondary organic aerosol formed. Experiments were conducted using a smog chamber operated in a steady-state mode permitting measurements of moderately low aerosol levels. GC-MS analysis was conducted to measure methyl butenediols in the gas phase and polyols in the aerosol phase. Analyses were made to obtain several bulk aerosol parameters from the reaction including values for the organic mass to organic carbon ratio, the effective enthalpy of vaporization (ΔHvapeff), organic peroxide fraction, and the aerosol yield. The gas phase analysis showed the presence of methacrolein, methyl vinyl ketone, and four isomers of the methyl butenediols. These gas-phase compounds may serve as precursors for one or more of several compounds detected in the aerosol phase including 2-methylglyceric acid, three 2-methyl alkenetriols, and two 2-methyl tetrols. In contrast to most previous studies, the 2-methyl tetrols (and the 2-methyl alkenetriols) were found to form in the absence of acidic sulfate aerosol. However, reaction conditions did not favor the production of HO2 radicals, thus allowing RO2+RO2 reactions to proceed more readily than if higher HO2 levels had been generated. SOA/SOC (i.e. OM/OC) was found to average 1.9 in the absence of NOx. The effective enthalpy of vaporization was measured as 38.6 kJ mol−1, consistent with values used previously in modeling studies. The yields in this work (using an independent technique than used previously) are lower than those of Kroll et al. (2006) for similar aerosol masses. SOC yields reported in this work range from 0.5–1.4% for carbon masses between 17 and 49 μgC m−3.
Highlights
Emissions of isoprene (C5H8) from vegetation constitute the greatest worldwide source of nonmethane hydrocarbons (Guenther et al, 1995)
Emphasis is placed on studying secondary organic aerosol (SOA) formation from the photooxidation of isoprene in the absence of nitrogen oxides (NOx), since isoprene aerosol does not appear to form until RO2+HO2 reactions become important (Dommen et al, 2006). As part of this effort, we have examined the relationship of the gas-phase intermediates to the isoprene tracer compounds formed during irradiation and whether acidic sulfate aerosol is essential for the formation of the 2-methyl tetrols
For experiments without NOx, the photolysis of H2O2 was the only source of OH, since OH cannot be generated by catalytic means in these types of photochemical systems without involving NOx
Summary
Emissions of isoprene (C5H8) from vegetation constitute the greatest worldwide source of nonmethane hydrocarbons (Guenther et al, 1995). While it is well known that isoprene has a strong influence on levels of atmospheric gas-phase oxidants, it has only been determined recently that isoprene plays a role in secondary organic aerosol (SOA) formation in the ambient atmosphere. Claeys et al (2004a) deduced the presence of isoprene SOA by detecting two polyols, 2methylthreitol and 2-methylerythritol, from filter samples of particulate matter taken in the Amazon rainforest. The methyl tetrols were used as tracer compounds to estimate the contribution of SOA from isoprene in several different ambient areas worldwide (Kleindienst et al, 2007b; Lewandowski et al, 2008; Hu et al, 2008). Secondary organic aerosol from the photooxidation of isoprene has been examined in a limited number of laboratory studies in the presence and absence of oxides of nitrogen (NOx).
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.